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024 7 _ |2 DOI
|a 10.1016/j.ecolmodel.2008.02.007
024 7 _ |2 WOS
|a WOS:000256608000015
037 _ _ |a PreJuSER-62049
041 _ _ |a eng
082 _ _ |a 570
084 _ _ |2 WoS
|a Ecology
100 1 _ |a Herbst, M.
|b 0
|u FZJ
|0 P:(DE-Juel1)129469
245 _ _ |a Multiyear heterotrophic soil respiration: Evaluation of a coupled CO2 transport and carbon turnover model
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2008
300 _ _ |a 271 - 283
336 7 _ |a Journal Article
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336 7 _ |a article
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440 _ 0 |a Ecological Modelling
|x 0304-3800
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|v 214
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Modelling of soil respiration plays an important role in the prediction of climate change. Soil respiration is usually divided in a fraction originating from root respiration and a heterotrophic fraction originating from microbial decomposition of soil organic carbon. This paper reports on the coupling of an one-dimensional water, heat and CO2 flux model (SOILCO2) with a pool concept of carbon turnover (RothC) for the prediction of soil heterotrophic respiration. In order to test this coupled model, it was applied to a bare soil experimental plot located in Bornim, Germany. Soil temperature and soil water content measurements were used for comparison with the respective model predictions. An 8 years data set Of CO2 efflux measurements, covering a broad range of atmospheric conditions, was used to evaluate the model. In a first step we quantified the improvement of the CO2 efflux prediction due to the coupling of the flux model with a pool concept of carbon turnover. The humus pool decomposition rate constant and its soil water content dependent reduction were derived from the first 5 years Of CO2 efflux measurements using inverse modelling. The following 3 years of measurements were used to validate the model. The overall model performance Of CO2 efflux predictions was acceptable with the measured and simulated mean daily respiration being 0.861 and 0.868 g C m(-2) d(-1), respectively, and a mean absolute difference between modelled and measured rates of 0.21 g C m(-2) d(-1). The inverse estimation of the humus decomposition rate constant resulted in a value of 0.04 year(-1), which is higher than the default value in RothC. This is attributed to the agricultural practice during the experiment. (c) 2008 Elsevier B.V. All rights reserved.
536 _ _ |a Terrestrische Umwelt
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588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a J
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653 2 0 |2 Author
|a soil organic carbon
653 2 0 |2 Author
|a heterotrophic soil respiration
653 2 0 |2 Author
|a model
653 2 0 |2 Author
|a SOILCO2
653 2 0 |2 Author
|a RothC
700 1 _ |a Hellebrand, H. J.
|b 1
|u FZJ
|0 P:(DE-Juel1)VDB72388
700 1 _ |a Bauer, J.
|b 2
|u FZJ
|0 P:(DE-Juel1)VDB62716
700 1 _ |a Huisman, J. A.
|b 3
|u FZJ
|0 P:(DE-Juel1)129472
700 1 _ |a Simunek, J.
|b 4
|u FZJ
|0 P:(DE-Juel1)VDB57645
700 1 _ |a Weihermüller, L.
|b 5
|u FZJ
|0 P:(DE-Juel1)VDB17057
700 1 _ |a Graf, A.
|b 6
|u FZJ
|0 P:(DE-Juel1)129461
700 1 _ |a Vanderborght, J.
|b 7
|u FZJ
|0 P:(DE-Juel1)129548
700 1 _ |a Vereecken, H.
|b 8
|u FZJ
|0 P:(DE-Juel1)129549
773 _ _ |a 10.1016/j.ecolmodel.2008.02.007
|g Vol. 214, p. 271 - 283
|p 271 - 283
|q 214<271 - 283
|0 PERI:(DE-600)2000879-X
|t Ecological modelling
|v 214
|y 2008
|x 0304-3800
856 7 _ |u http://dx.doi.org/10.1016/j.ecolmodel.2008.02.007
909 C O |o oai:juser.fz-juelich.de:62049
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